首页> 美国卫生研究院文献>Journal of Visualized Experiments : JoVE >Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
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Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt

机译:地下火山3D地震成像的数据处理方法:在塔里木洪水玄武岩中的应用

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摘要

The morphology and structure of plumbing systems can provide key information on the eruption rate and style of basalt lava fields. The most powerful way to study subsurface geo-bodies is to use industrial 3D reflection seismological imaging. However, strategies to image subsurface volcanoes are very different from that of oil and gas reservoirs. In this study, we process seismic data cubes from the Northern Tarim Basin, China, to illustrate how to visualize sills through opacity rendering techniques and how to image the conduits by time-slicing. In the first case, we isolated probes by the seismic horizons marking the contacts between sills and encasing strata, applying opacity rendering techniques to extract sills from the seismic cube. The resulting detailed sill morphology shows that the flow direction is from the dome center to the rim. In the second seismic cube, we use time-slices to image the conduits, which corresponds to marked discontinuities within the encasing rocks. A set of time-slices obtained at different depths show that the Tarim flood basalts erupted from central volcanoes, fed by separate pipe-like conduits.
机译:管道系统的形态和结构可以提供有关玄武岩熔岩田的喷发率和样式的关键信息。研究地下地质体的最有效方法是使用工业3D反射地震成像。但是,对地下火山成像的策略与油气藏的策略非常不同。在这项研究中,我们处理了来自中国塔里木盆地北部的地震数据立方体,以说明如何通过不透明度渲染技术可视化窗台以及如何通过时间切片对管道进行成像。在第一种情况下,我们通过标记视线和围岩层之间的接触的地震视界来隔离探针,应用不透明度渲染技术从地震立方体中提取视线。所得的详细门槛形态表明流向是从穹顶中心到边缘。在第二个地震立方体中,我们使用时间切片对导管进行成像,这与围岩中明显的不连续性相对应。在不同深度获得的一组时间切片显示,塔里木洪水玄武岩由中央火山喷发,由分开的管状导管提供。

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